waves 1
Introduction to Waves and Oscillatory Motion
Review of Simple Harmonic Motion (SHM):
A body performs oscillatory motion about a specific point known as the Mean Point or Equilibrium Point.
At the mean point, the net force acting on the body is zero ().
Simple Harmonic Motion is defined by the proportionality: .
The motion is characterized as vibratory, to-and-fro, and periodic.
The restoring force is directly proportional to the negative of the displacement.
Definition of a Wave:
A wave is fundamentally a disturbance in a medium that propagates from one point to another.
Propagation refers to the movement of this disturbance between two points (e.g., from Point A to Point B).
Conceptually, a wave is a mechanism for the transport of energy.
Analogy: Like a courier service (TCS) delivering a parcel from one point to another, a wave delivers energy without the bulk movement of the medium itself.
Energy Categorization:
Progressive Wave: A wave that carries and transfers energy from one point to another as it moves forward.
Non-Progressive / Standing / Stationary Wave: A wave where energy is not transferred between points (to be discussed later).
Classification of Waves Based on Particle Vibration
Transverse Waves:
In these waves, the particles of the medium vibrate perpendicular to the direction of wave propagation.
Mechanism: If energy moves horizontally, the particles move up and down.
Example: A wave in a stretched string. When a jerk is given to one end of a rope, the pulse (energy) moves forward, but individual points on the rope (e.g., Point X or Point Y) only move up and down at their original locations.
Other examples include light waves (electromagnetic waves) and ripple tank waves (water ripples).
These waves consist of Crests (camels-hump-like structures) and Troughs (valley-like structures).
Longitudinal Waves:
In these waves, the particles of the medium vibrate parallel or along the same line as the direction of wave propagation.
Mechanism: Particles undergo to-and-fro motion in the same direction as the energy flow.
Example: Sound waves in air. When sound is produced, air particles collide with neighbors, transmitting energy forward and returning to their original positions.
Other examples include waves in a Slinky Spring.
These waves consist of Compressions (particles close together, high pressure, high density) and Rarefactions (particles spread out, low pressure, low density).
Classification Based on Medium Requirement
Mechanical Waves:
These require a material medium for propagation because they rely on particle interaction.
Example: Sound waves.
The Bell Jar Experiment:
An electric bell is placed inside a jar. As air is pumped out using a vacuum pump, the sound of the bell fades until it becomes silent, even though the hammer continues to strike the gong. This proves sound cannot travel through a vacuum.
Non-Mechanical (Electromagnetic) Waves:
These do not require a material medium and can travel through a vacuum.
Examples include the electromagnetic spectrum: Radio waves, Microwaves, Infrared, Visible light, Ultraviolet, X-rays, and Gamma rays.
These are composed of energy packets called photons.
In a vacuum, they all travel at the speed of light: .
Basic Wave Characteristics and the Wave Equation
Wave Cycle Representation:
One wave cycle is completed when a particle of the medium finishes one full oscillation (goes from mean to positive extreme, then to negative extreme, and back to mean).
A wave cycle corresponds to a phase change of or .
Fundamental Quantities:
Wavelength (): The length of one complete wave cycle.
Frequency (): The number of waves passing through a point in one second ().
Time Period (): The time required for one complete wave to pass a point ().
Wave Velocity (): Derived from . For one cycle, and , leading to or the standard wave equation:
Medium Transition Rule:
When a wave moves from Medium 1 to Medium 2, its velocity () and wavelength () change.
The frequency () remains constant because it depends solely on the source of the disturbance.
Concepts of Phase and Path Difference
Phase ():
Phase describes the instantaneous behavior (position and direction of motion) of a vibrating particle.
In-Phase Points: Points that have the same displacement and are moving in the same direction at the same time (e.g., two crests). The phase difference is an even multiple of (i.e., ).
Out-of-Phase Points: Points where the behavior is different. If they are exactly opposite (e.g., a crest and a trough), they are or out of phase.
Mathematical Relationship:
The relationship between phase difference () and path difference () is given by:
Example: If the path difference is , the phase difference is:
Velocity of Sound: Newton's Formula and Laplace Correction
Newton’s Theoretical Approach:
Newton proposed that velocity depends on the elastic property (, Bulk Modulus) and inertial property (, density) of the medium:
Assumption: Sound propagation is an isothermal process (temperature remains constant because heat has time to flow from compressions to rarefactions).
For gases, Newton replaced Bulks Modulus () with Pressure (), resulting in:
Result: At , Newton calculated .
Error: The experimental value was . Newton's value had an approximate 16% error.
Laplace Correction:
Laplace argued that the process is adiabatic, not isothermal.
Reasoning: Sound travels so fast that there is no time for heat exchange (thermal contact is not established). Also, air is a poor conductor of heat.
For an adiabatic process, the Bulk Modulus is , where .
Formula:
For air (diatomic), . Calculating at gives , which matches experimental data.
Factors Affecting the Speed of Sound
Temperature:
Speed is directly proportional to the square root of the absolute temperature ( in Kelvin):
Relationship:
Approximate Temperature Formula: For small changes in temperature (up to ):
Here, and is the temperature in degrees Celsius.
Pressure:
Speed of sound does not depend on pressure change alone because a change in pressure causes a proportional change in density, keeping the ratio constant.
Medium Type:
Sound travels fastest in solids, then liquids, and slowest in gases (v_{solid} > v_{liquid} > v_{gas}) because solids have much higher elasticity ().
Principle of Superposition and Interference
Principle of Superposition:
When two or more waves meet at a point, the net displacement () is the vector sum of the individual displacements:
Wave Interference:
Constructive Interference:
Occurs when waves meet in-phase (Crest meets Crest, Trough meets Trough).
Resultant intensity and amplitude are maximized.
Path difference: (where ).
Phase difference: (even multiples of ).
Results in lauder sound or brighter light.
Destructive Interference:
Occurs when waves meet out-of-phase (Crest meets Trough).
Resultant intensity and amplitude are minimized.
Path difference: or odd multiples of .
Phase difference: (odd multiples of ).
Results in fainter sound or darker spots.
Intensity Calculation:
Intensity () is proportional to the square of the amplitude ().
Max Intensity: .
Min Intensity: .